Hostname: page-component-cd9895bd7-gbm5v Total loading time: 0 Render date: 2024-12-19T01:58:45.757Z Has data issue: false hasContentIssue false

A Method for the Analysis of Transient Motion of a Kelvin-Voigt Half-Space

Published online by Cambridge University Press:  05 May 2011

Chau-Shioung Yeh*
Affiliation:
Dept. of Civil Engineering, Institute of Applied Mechanics, National Taiwan University, Taipei, Taiwan 10617, R.O.C.
Wen-I Liao*
Affiliation:
Dept. of Civil and Environmental Engineering, National Kaohsiung University, Kaohsiung, Taiwan 820, R.O.C.
Tsung-Jen Teng*
Affiliation:
National Center for Research on Earthquake Engineering, Taipei, Taiwan 106, R.O.C.
Wen-Shinn Shuy*
Affiliation:
Department of Civil Engineering, National Taiwan University, Taipei, Taiwan 10617, R.O.C.
*
* Professor
** Assistant Professor
*** Research Fellow
**** Formerly graduate student
Get access

Abstract

In this paper, a modified version of method of steepest descent combining with Durbin's method is proposed to study the transient motion in either an elastic or a viscoelastic half-space. The causal condition is satisfied based on the Durbin's method while the wavenumber integral for any range of frequency is evaluated by applying the modified method of steepest descent. The validity and accuracy of the proposed method is tested by studying the transient response generated by a buried dilatational line source in an elastic half-space, for which the exact solution (Garvin's solution) can be obtained. Then the same formalism is extended to Kelvin-Voigt half-space, and the transient surface motions in elastic or viscoelastic half-spaces media are studied and discussed in details.

Type
Articles
Copyright
Copyright © The Society of Theoretical and Applied Mechanics, R.O.C. 2003

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

1Spencer, T. W., “The Method of Generalized Reflection and Transmission Coefficients,” Geophysics, 25, pp. 625641 (1960).CrossRefGoogle Scholar
2Müller, G., “Theoretical Seismogram for Some Types of Point Sources in Layered Media, Part III, Single Force and Dipole Sources of Arbitrary Orientation,” Z. Geophys., 35, pp. 347371 (1969).Google Scholar
3Pao, Y. H. and Gajewski, R. R., “The Generalized Ray Theory and Transient Response of Layered Elastic Solids,” Physical Acoustics, Mason, W. P. and Thurston, R. N., ed., 13, Academic Press, New York (1977).Google Scholar
4Borejko, P. and Ziegler, F., “Surface Waves on an Isotropic Viscoelastic Half-Space: the Method of Generalized Rays,” Recent Developments in Surface Acoustic Waves, Parker, D. F. and Maugin, G. A., ed., Springer-Verlag, pp. 299308 (1988).CrossRefGoogle Scholar
5Bland, D. R., The Theory of Linear Viscoelasticity, Pergamon Press, Oxford (1960).Google Scholar
6Bouchon, M. and Aki, K., “Discrete Wave-Number Representation of Seismic-Source Wave Field,” Bull. Seism. Soc. Am., 67(2), pp. 259277 (1977).CrossRefGoogle Scholar
7Garvin, W.,“Exact Transient Solution for the Buried Line Source Problem,” Proc. Roy. Soc. London, A203, pp. 528541 (1956).Google Scholar
8Durbin, F., “Numerical Inversion of Laplace Transforms, an Efficient Improvement to Dubner and Abate's Method,” The Computer Journal, 17(4), pp. 371376 (1974).CrossRefGoogle Scholar
9Narayanan, G. V. and Beskos, D. E., “Numerical Operational Methods for Time-Dependent Linear Problems,” International Journal for Numerical Methods in Engineering, 18, pp. 18291854 (1982).CrossRefGoogle Scholar
10Ewing, W. M., Jardetzky, W. S. and Press, F., Elastic Waves in Layered Media, McGraw-Hill, New York (1957).CrossRefGoogle Scholar
11Yeh, C. S., Teng, T. J. and Liao, W. I., “On Evaluation of Lamb's Integrals for Waves in a Two-Dimensional Elastic Half-Space,” The Chinese Journal of Mechanics, 16(2), pp. 109124 (2000).CrossRefGoogle Scholar